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The flushing time in an estuary is important for water quality analysis, and it is one of the major transport time scales used in estuaries to quantify the hydrodynamic processes and for water resources management strategies. The purpose of this paper is to investigate the influence of tidal amplitude, river discharge, and salinity stratification on the spatially varying flushing time of the two selected Moroccan Atlantic semi-closed estuaries, i.e. Bouregreg and Loukkos. A freshwater fraction method (FFM) was used to calculate flushing time for both estuaries using a spatially varying freshwater fraction. The results showed that the flushing time varies from 2.7 to 6.3 days for a river discharge ranges from 17 to 22 m 3 s −1  during spring tide, and from 3.4 to 11.2 days for a river discharge ranges from 17 to 31 m 3 s −1  during neap tide in Bouregreg estuary, and varies from 10 to 13.6 days for a river discharge ranges from 3.47 to 5.12 m 3 s −1  during spring tide, and from 9.11 to 13.1 days for a river discharge ranges from 3.47 to 5.48 m 3 s −1  at neap tide in Loukkos estuary. In addition, the flushing time near the mouth for both estuaries is shorter during spring tide than during neap tide because of the larger amplitude of the spring tide. At the estuary mouth (e.g. Bouregreg estuary), the potential energy anomaly of the water column is negligible (&lt;4 J m −3 ).

The calculation of estuarine flushing times in convergent estuaries using fresh-water fraction method